
sedimentary
Sandstone (Weathered Cobble)
Clastic sedimentary rock (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale (due to quartz content); Color: Tan, beige, grey, with traces of green lichen; Luster: Dull/Earthy; Crystal Structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 on Mohs scale (due to quartz content)
- Color
- Tan, beige, grey, with traces of green lichen
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale (due to quartz content); Color: Tan, beige, grey, with traces of green lichen; Luster: Dull/Earthy; Crystal Structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. This specific specimen is a 'glacial cobble' or river rock, rounded by mechanical weathering and transport over thousands of years.
Uses & applications
Commonly used in construction as aggregate, for paving, or as decorative garden stones. High-purity sandstone is used in glass manufacturing.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. This specific rock shows signs of biological weathering on its surface, indicated by the small green patches of lichen growth.
Field identification & locations
Identify in the field by its gritty, sandpaper-like texture and visible grain structure. This specimen is a common 'erratic' or river-worn cobble found throughout temperate regions in Northern North America and Europe.
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